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The Acoustic Properties of Sandy and Clayey Hydrate-Bearing Sediments

Author

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  • Xiao-Hui Wang

    (State Key Laboratory of Heavy Oil Processing, China University of Petroleum, Beijing 102249, China)

  • Qiang Xu

    (State Key Laboratory of Heavy Oil Processing, China University of Petroleum, Beijing 102249, China)

  • Ya-Nan He

    (State Key Laboratory of Heavy Oil Processing, China University of Petroleum, Beijing 102249, China
    Department of Pharmacy, Cangzhou Medical College, Cangzhou 061001, China)

  • Yun-Fei Wang

    (State Key Laboratory of Heavy Oil Processing, China University of Petroleum, Beijing 102249, China)

  • Yi-Fei Sun

    (State Key Laboratory of Heavy Oil Processing, China University of Petroleum, Beijing 102249, China)

  • Chang-Yu Sun

    (State Key Laboratory of Heavy Oil Processing, China University of Petroleum, Beijing 102249, China)

  • Guang-Jin Chen

    (State Key Laboratory of Heavy Oil Processing, China University of Petroleum, Beijing 102249, China)

Abstract

Natural gas hydrates samples are rare and difficult to store and transport at in situ pressure and temperature conditions, resulting in difficulty to characterize natural hydrate-bearing sediments and to identify hydrate accumulation position and saturation at the field scale. A new apparatus was designed to study the acoustic properties of seafloor recovered cores with and without hydrate. To protect the natural frames of recovered cores and control hydrate distribution, the addition of water into cores was performed by injecting water vapor. The results show that hydrate saturation and types of host sediments are the two most important factors that govern the elastic properties of hydrate-bearing sediments. When gas hydrate saturation adds approximately to 5–25%, the corresponding P-wave velocity ( V p ) increases from 1.94 to 3.93 km/s and S-wave velocity ( V s ) increases from 1.14 to 2.23 km/s for sandy specimens; V p and V s for clayey samples are 1.72–2.13 km/s and 1.10–1.32 km/s, respectively. The acoustic properties of sandy sediments can be significantly changed by the formation/dissociation of gas hydrate, while these only minorly change for clayey specimens.

Suggested Citation

  • Xiao-Hui Wang & Qiang Xu & Ya-Nan He & Yun-Fei Wang & Yi-Fei Sun & Chang-Yu Sun & Guang-Jin Chen, 2019. "The Acoustic Properties of Sandy and Clayey Hydrate-Bearing Sediments," Energies, MDPI, vol. 12(10), pages 1-11, May.
    • Handle: RePEc:gam:jeners:v:12:y:2019:i:10:p:1825-:d:230927
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    References listed on IDEAS

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    1. Bei Liu & Heng Pan & Xiaohui Wang & Fengguang Li & Changyu Sun & Guangjin Chen, 2013. "Evaluation of Different CH 4 -CO 2 Replacement Processes in Hydrate-Bearing Sediments by Measuring P-Wave Velocity," Energies, MDPI, vol. 6(12), pages 1-13, November.
    2. Dongliang Li & Qi Wu & Zhe Wang & Jingsheng Lu & Deqing Liang & Xiaosen Li, 2018. "Tri-Axial Shear Tests on Hydrate-Bearing Sediments during Hydrate Dissociation with Depressurization," Energies, MDPI, vol. 11(7), pages 1-12, July.
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    Cited by:

    1. Lin Liu & Xiumei Zhang & Xiuming Wang, 2021. "Wave Propagation Characteristics in Gas Hydrate-Bearing Sediments and Estimation of Hydrate Saturation," Energies, MDPI, vol. 14(4), pages 1-21, February.

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